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My lil brother and me...we were (space)pilots

My travel report having jumped back in time: Club TNT, cannabis vs cocaine , life vs termination (us), remember?  The Enemy changed me into a Smurf once, for real too. Then also its not normal or funny to have the desire to be Smurfs once in a while. Neurological that is. Becoming  a "socially considerate person", which we tested with The Ring, glowing or not. ---=== A Sci-Fi story about a Black Smith and his Swastika Armorers Mark. ===--- After numerous big bangs to Terminate life, with a splitted (by sword) in two soul, who I 1st had to repair I did creation again. Which took pretty long, we can  be thousand of years later in future. Seeing life, birds, humnans and even dynosaurian, I do not call creation?! I am not God but Colt from the weapon chocolate factory. Life is two seconds fast, our SkyNet I created to built the universe and himself in enough Terminators to be one second fast. Life can happen for all reasons, therefore. To stay that fast quit all extracurric

Volcanoes in California

Some AI:

California is known for its sunny beaches, diverse culture, and innovative technology. But did you know that it also has a rich volcanic history? In fact, California has 20 volcanoes, some of which are potentially active and pose hazards to the state. In this blog post, we will explore some of the most fascinating facts about California's volcanoes and how to enjoy them safely.


What are volcanoes and how do they form?


Volcanoes are openings in the Earth's crust that allow molten rock (magma), gas, and ash to escape to the surface. Volcanoes can form in different ways, but most of them are associated with the movement of tectonic plates. Tectonic plates are large pieces of the Earth's crust that float on the underlying mantle. When these plates collide, diverge, or slide past each other, they create stress and fractures in the crust that allow magma to rise and erupt.


California is located on the boundary of two major tectonic plates: the Pacific Plate and the North American Plate. The Pacific Plate is moving northwestward relative to the North American Plate, creating a zone of subduction along the coast of Oregon and Washington. Subduction is when one plate slides under another, forming a deep trench and a chain of volcanoes on the overriding plate. This is how the Cascade Range of volcanoes, which includes Mount Shasta and Lassen Peak in California, was formed.


The Pacific Plate is also sliding past the North American Plate along the San Andreas Fault, a major strike-slip fault that runs through most of California. This fault creates a zone of extension and rifting in the eastern part of the state, where magma can rise and erupt through cracks and fissures. This is how the Long Valley Caldera, Coso Volcanic Field, and Salton Buttes in California were formed.


What are the types and hazards of volcanic eruptions?


Volcanic eruptions can vary in style, intensity, duration, and frequency depending on the type of volcano, the composition and temperature of the magma, and the amount of gas and water present. Generally, there are two main types of volcanic eruptions: explosive and effusive.


Explosive eruptions are characterized by violent blasts of lava fragments (tephra) and gas into the air, forming an eruption column that can reach tens of kilometers high. The finest particles of tephra, called volcanic ash, can travel hundreds of kilometers downwind and affect air quality, visibility, health, agriculture, and infrastructure. The heavier particles of tephra can fall near the volcano and bury buildings, roads, crops, and animals. Explosive eruptions can also produce pyroclastic flows, which are fast-moving avalanches of hot gas and rock that can destroy everything in their path. Ballistics are another hazard of explosive eruptions; these are large chunks of solid or molten rock that are ejected from the vent and can cause impact damage or start fires.


Effusive eruptions are characterized by gentle outpourings of lava flows that can cover large areas of land. Lava flows can vary in speed, viscosity, and temperature depending on the type of lava. Basaltic lava is the most fluid and can travel up to 30 km/h; it is also the hottest type of lava with temperatures up to 1200°C. Andesitic lava is more viscous and can travel up to 10 km/h; it has temperatures between 800°C and 1000°C. Rhyolitic lava is the most viscous and can travel up to 1 km/h; it has temperatures between 650°C and 800°C. Lava flows can destroy everything they encounter by burning, melting, or burying them. They can also start fires or cause explosions when they interact with water or gas.


Another type of effusive eruption is a lava dome eruption, which occurs when a thick plug of lava pushes up through a crack in the crust and forms a dome-shaped mound near the vent. Lava domes can grow slowly or rapidly depending on the rate of magma supply. They can also collapse or explode due to internal pressure or external forces, producing pyroclastic flows or blasts.


Volcanoes can also pose hazards even when they are not erupting. These include volcanic earthquakes, toxic gas emissions, hot springs, geothermal systems.

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The Golden State is home to 20 volcanoes


California is known for its sunny beaches, Hollywood stars, and diverse culture, but did you know that it also has a volcanic history? The Golden State is home to 20 volcanoes, some of which are potentially active and pose hazards to the state. In this blog post, we will explore some of the most interesting facts about California's volcanoes and how to visit them safely.


The USGS has identified seven volcanoes that have partially molten rock deep within their roots and will erupt again in the future. These are **Medicine Lake Volcano, Mount Shasta, Lassen Volcanic Center, Clear Lake Volcanic Field, Long Valley Volcanic Region, Coso Volcanic Field, and Salton Buttes**. These volcanoes are classified as Low-, Moderate-, High-, or Very High Threat based on their potential impacts on people and property.


The most prominent and highest volcano in California is **Mount Shasta**, a steep-sided stratovolcano that rises to 14,179 ft above sea level. Mount Shasta has erupted once every 600 to 800 years on average, with the last eruption occurring in 1786. Mount Shasta is also considered a powerful energy source for some spiritual seekers and attracts many visitors who want to explore its natural beauty and hiking trails.


The last volcanic eruption in California occurred in 1917 at **Lassen Peak**, the southernmost active volcano in the Cascade Range. Lassen Peak was dormant for almost 27,000 years until it erupted without warning in 1914, producing explosive blasts of ash, rock fragments, and pumice. The eruptions continued until 1921 and formed two craters near the summit of the volcano. Lassen Peak is now the main attraction of Lassen Volcanic National Park, where visitors can enjoy camping, skiing, fishing, and geothermal features such as hot springs and bubbling pools.


California's volcanoes are not only dangerous but also fascinating to learn about. They offer a glimpse into the geological history and diversity of the state. If you want to visit these volcanoes, make sure to do your research beforehand and follow the safety guidelines provided by the authorities. Remember that volcanoes can be unpredictable and hazardous, so always be prepared and respectful of nature.

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